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- W972906859 endingPage "662" @default.
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- W972906859 abstract "The water content, solution phase content, or wetness of the soil may be expressed on a weight, volume, or degree of saturation basis. For analysis of water flow in soil profiles, the volume basis is most useful. The water retention function is primarily dependent upon the texture or particle-size distribution of the soil, and the structure or arrangement of the particles. The soil-water system is in hydraulic contact with the body of water via a water-wetted porous plate or membrane. Water retention measurements on subsoils, especially those in which there is a significant degree of structural development, should be made on undisturbed core samples. The chemical composition of the wetting fluid can affect the water retention of the samples, particularly in fine-textured soils that contain significant amounts of swelling clays. The intensity of the forces retaining the water in the soil at a given matric pressure head is temperature-dependent." @default.
- W972906859 created "2016-06-24" @default.
- W972906859 creator A5048983491 @default.
- W972906859 date "2018-09-11" @default.
- W972906859 modified "2023-10-16" @default.
- W972906859 title "Water Retention: Laboratory Methods" @default.
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- W972906859 doi "https://doi.org/10.2136/sssabookser5.1.2ed.c26" @default.
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